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and Webb, 1990) Sediments in the vicinity of the site generally consist of reddish- <br /> brown to dark gray clayey silt with moderate to well sorted, fine sand lenses <br /> The Central Valley is drained by two large river systems- the Sacramento River <br /> (northern part of the Valley) and the San Joaquin River (most of the southern part of <br /> the Valley). The two rivers meet about 13.6 miles northwest of the facility The <br /> closest surface water features are the easternmost reach of the Port of Stockton, <br /> approximately 1,000 feet north-northwest of the facility, and Mormon Slough, located <br /> approximately 1,300 feet southwest of the facility (Figure 1) <br /> Historically, groundwater in the Stockton area has typically occurred under water /?f( <br /> table conditions at a depth between25 and 35 feet (Infurna, 1991). Severe drought <br /> conditions during recent years combined with the intense agricultural development have <br /> lowered the water table to below 40 feet. <br /> ' Groundwater flow direction in the area is influenced primarily by the Port of <br /> Stockton Channel Influence by the smaller Mormon Slough is expected to be <br /> seasonal, moving laterally away from the Slough during high precipitation periods. <br /> ' Based on water level measurements taken on August 30, 1994, the present depth to <br /> water at the facility is approximately 41 feet. Groundwater flow is to the south with a <br /> hydraulic gradient of 0.003 feet Mr foot. <br /> ' Local Surface Water and Groundwater Use <br /> The City of Stockton obtains its municipal and industrial water supplies from a <br /> combination of treated surface water and numerous groundwater supply wells located in <br /> and around Stockton. According to the State of California, Department of Water <br /> Resources well records, no domestic or mtable water supply wells are located within 1 <br /> mile of the Greyhound facility <br /> ' SITE NVESTIGATION <br /> Soil Boring and Soil Sampling Procedures <br /> ' In August 1994, a total of eight additional soil borings (SB-1 through SB-8) were <br /> advanced at the locations shown on Figure 2 to characterize the lateral and vertical <br /> ' extent of hydrocarbon contamination at the site. Each of the borings was advanced to <br /> depths between 45 and 51.5 feet using 4 25-inch inside-diameter hollow-stem augers <br /> and split-spoon sampling techniques in accordance with ASTM-Standard D-1586. <br /> Prior to advancing each boring, all downhole equipment was decontaminated by steam- <br /> cleaning. All drill cuttings were containerized in labeled DOT-approved, 55-gallon <br /> drums, and left on-site for proper disposal by Greyhound at a later date. <br /> Soil samples were collected for laboratory analysis in 6-inch long brass sample <br /> tubes that were inserted into a 1.5-foot-long split-spoon sampler at 5-foot intervals. <br /> Soil sampling protocol consisted of capping each end of the brass tube with teflon tape <br /> and non-reactive, plastic end-caps The caps were then sealed with clear tape. A <br /> chain-of-custody record accompanied each soil sample container from selection and <br /> preparation at the laboratory, during sample collection at the site, and through analysis <br /> at the laboratory Each sample was individually labeled, identified in the field <br /> notebook, immediately packed in ice, sealed inside an insulated shipping container, and <br /> PAMSYROBVOLI WAM386 08969125386R02 DOC <br />